Tim Horner CSUS Geology Department

1. Streams and FloodsPhysical Geology, Chapter 10 Tim Horner CSUS Geology Department

2. Running Water • Running wateris the most important geologic agent in eroding, transporting and depositing sediment • Nearly every landscape on Earth shows the results of stream erosion or deposition

3. Hydrologic Cycle • Hydrologic cycle - the movement and interchange of water between the sea, air, and land • Evaporation • Solar radiation provides energy • Precipitation • Rain or snow • Transpiration • Evaporation from plants • Runoff • Water flowing over land surface • Infiltration • Water soaking into the ground

4. Running Water • Stream - a body of running water, confined to a channel, that runs downhill under the influence of gravity • Headwaters - upper part of stream near its source in the mountains • Mouth - place where a stream enters sea, lake or larger stream • Channel - a long, narrow depression eroded by a stream into rock or sediment • Stream banks - sides of channel • Streambed - bottom of the channel • Floodplain - flat valley floor composed of sediment deposited by the stream

5. Drainage Basins • Drainage basin - the total area drained by a stream and its tributaries • Tributary - a small stream flowing into a larger one • Divide - ridge or high ground that divides one drainage basin from another • Continental Divide separates the streams that flow into the Pacific from those that flow into the Atlantic and Gulf of Mexico

6. Drainage Patterns • Drainage pattern - the arrangement, in map view, of a stream and its tributaries • Most tributaries join the main stream at an acute angle, forming a V or Y pointing downstream • Dendritic - drainage pattern resembling the branches of a tree • Radial pattern - streams diverge outward like the spokes of a wheel • Typically form on conical mountains (volcanoes) • Rectangular pattern - tributaries have frequent 90° bends and join other streams at right angles • Trellis pattern - parallel streams with short tributaries meeting at right angles

7. Stream Erosion • Stream erosion (and deposition) controlled by flow velocity and discharge • Stream velocity controlled by stream gradient (slope), channel shape and channel roughness • Maximum velocity near center of channel • Floods involve increased velocity and discharge (volume of water passing a particular point in a stream over time) • Higher stream velocities promote erosion and transport of coarser sediments • Erosion of very small particles difficult due to molecular binding forces

8. Stream Erosion • Streamgradient is the downhill slope of the streambed • Typically measured in feet per mile in the U.S., and in meters per kilometer elsewhere • Usually decreases downstream • Channel shape and roughness • Both effect stream velocity due to drag • Narrower, deeper channels allow faster flow • Smoother channels allow faster flow • Wider, shallower channels decrease flow speed • Rougher channels decrease flow speed • Stream discharge is the volume of water flowing past a given point in a unit of time

9. Stream Erosion • Streams cut their own valleys, deepening and widening them over time and carrying away the sediment • Stream erosion occurs by three mechanisms: hydraulic action, solution, and abrasion • Hydraulic action - ability of flowing water to pick up and move rock and sediment • Solution - dissolving of rocks (e.g., limestone) • Abrasion - grinding away of stream channel by the friction and impact of the sediment load • Potholes are eroded into streambed by the abrasive action of the sediment load in the stream

10. Sediment Deposition • Sediments are temporarily deposited along stream course as bars and floodplain deposits • Bars - ridges of sediment (usually sand or gravel) deposited in the middle or along the sides of a stream • Braided streams contain sediment deposited as numerous bars around which water flows in highly interconnected rivulets

11. Sediment Deposition • Meandering streams flow faster along the outside of bends and more slowly along the inside, depositing point bars on the insides of the meanders • Meander cutoffs may form when a new, shorter channel is cut through the narrow neck of a meander (as during a flood)

12. Sediment Deposition • Floodplains are broad strips of land built up by sedimentation on either side of a stream channel • Floodplain sediments are left behind as flood waters slow and recede at the end of flood events • Main channel has slightly raised banks with respect to the floodplain known as natural levees

13. Flooding • When water levels rise and overtop the banks of a river, flooding occurs • Natural process on all rivers • Described by recurrence intervals • A 100-year flood is, on average, the size of the largest flood within a 100-year period of time • Can cause great damage in heavily populated areas • High velocity and large volume of water causes flood erosion • Slowing of waters as flood ends causes flood deposits (usually of silt or clay-sized particles) to be deposited in the floodplain

14. Flooding • Urban flooding • Paved areas and storm sewers increase runoff by inhibiting infiltration • Rapid delivery of water to streams increases peak discharge and hastens occurrence of flood • Flash floods • Local, sudden floods of large volume and short duration • Typically triggered by heavy thunderstorms

15. Flooding • Flood control • Dams designed to trap flood waters in reservoirs upstream and release it gradually over time • Artificial levees designed to increase capacity of river channel • Works well until stream overtops artificially raised levees, leading to extremely rapid flooding and erosion • Wise land-use planning, including prevention of building within 100-year floodplains, is most effective

16. Sediment Transportation • Sediment load transported by a stream can be subdivided into bed load, suspended load, and dissolved load • Bed load - large or heavy particles that travel on the streambed • Traction load - large particles that travel along the streambed by rolling, sliding or dragging • Saltation load - medium particles (typically sand-sized) that travel downstream by bouncing along - sometimes in contact with the streambed and sometimes suspended in the flowing water • Suspended load - sediment that is small/light enough to remain above the stream bottom by turbulent flow for an indefinite period of time • Dissolved load - dissolved ions produced by chemical weathering of soluble minerals upstream

17. Sediment Deposition • Delta - body of sediment deposited at the mouth of a river when flow velocity decreases • Surface marked by shifting distributary channels • Shape of a delta depends on whether its wave-dominated, tide-dominated, or stream-dominated

18. Sediment Deposition • Alluvial fan - large, fan- or cone-shaped pile of sediment that forms where stream velocity decreases as it emerges from a narrow mountain canyon onto a flat plain • Well-developed in desert regions, such as the southwestern U.S. • Larger fans show grading from large sediments nearest the mountains to finer sediments farther away

19. Stream Valley Development • Downcutting • Process of deepening a valley by erosion of the streambed • V-shaped valleys typically form from downcutting combined with mass wasting and sheet erosion • Streams cannot erode below their base level • Basel level can be sea level, a lake, or the bottom of a closed basin (e.g., Death Valley, CA) • Downcutting rate can be rapid if a stream is well above base level (e.g., Grand Canyon, AZ)

20. Stream Valley Development • Graded streams • Characteristic concave-up longitudinal profile • Rapids and waterfalls have been smoothed out by extensive erosion over a long period of time • Delicate balance between available sediment load and transport capacity • Lateral erosion widens stream valleys by undercutting of stream banks and valley walls as stream swings from side to side across the valley floor • Headward erosion is the slow uphill growth of a valley above its original source by gullying, mass wasting, and sheet erosion

21. Stream Valley Development • Stream terraces • Step-like landforms found above a stream and its floodplain • Occurs when river rapidly cuts downward into its own floodplain • Represents relatively sudden change from deposition to erosion • Can be caused by rapid uplift, drops in base level, or climate changes

22. Stream Valley Development • Incised meanders • Retain sinuous pattern as they cut vertically downward • May be produced by profound base level changes, as when rapid tectonic uplift occurs

23. Stream Valleys on Mars • Evidence of different climate in past • Liquid water not stable on surface of Mars under present conditions • Too cold • Atmospheric pressure too low • Stream channels and terraces suggest long-term erosion by flowing water • Lack of smaller tributaries is puzzling, but these do exist for channels networks in more ancient terrains on Mars • Requires warmer, wetter Mars • NASA missions targeting such locations